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Minerals, Volume 8, Issue 11
November 2018 - 67 articles
Cover Story: Cover story: The coexistence of two-phase, vapor-rich, and polyphase, salt-saturated fluid inclusions in quartz is interpreted to indicate phase separation (i.e., a vapor and a dense liquid phase exsolved after brecciation occurred). The presence of halite, sylvite, and mica evidences salinities above 45 wt% NaCl eq.; magmatic-hydrothermal fluids trapped in quartz must have contained salts other than NaCl (e.g., KCl, CaCl2, and MgCl2). Deep-seated brine is the main ore-forming fluid responsible for mineralization at San Francisco de los Andes.View Paper here
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